Publications

Bochevar R.O. Formation accessory and creation stages of ore of ultrabasite massives of the Kapitanivske ore field // Scientific proceedings of the Institute of Geological Sciences of NAS of Ukraine. - № 4. – 2011 - С. 28-34.

Creation stages of ore of ultrabasite massives of the Kapitanivske ore field were extracted: magmatic, metamorphic, hydrothermal, supergene. Mineral associations creation stages of ore were described. Possible types of ores of investigation massives were determined. Formation accessory of ultrabasite massives of the Kapitanivske ore field is considered. Keywords: ultrabasite massif, ore formation, stages mineral origination, mineral association.

Kornienko P.K., Popovchenko S.E., Diachenko I.M., Vykhod M.K. Natural varieties of chromium ores in the Kapitanovskoe deposit and prospects of their platinum content // Scientific proceedings of the NSU. D.: State Higher Educational Institution «National Mining University». - № 40. - 2013. - P. 5–12.

The Kapitanovskoe deposit is considered as an object with primary development of platinumbearing chromium ores. The resources of PGE mineralization in chromite formation were estimated on the example of Kapitanovskoe deposit and the prospect of chromium-bearing ultramafic massifs in Middle Bug area is showed.

Pavliuk O.V., Kvasnytsya V.M., Kysliuk V.V., Pavliuk V.M. Native Platinum in Rocks of the Chemerpil’ska Structure (the Middle Bug Area) // Mineralogical Journal. - № 1. -32. - 2010. - C. 50-56.

Holovanivs’ka sutural zone attracts people attention of researchers the prospect region for elements of platinum group exploration for a long time. Starting from the 1970’s in the course of geological survey platinum anoma lies were explored in the North-Ternuvats’ka, Kapitans’ka, Lypovenkivs’ka and Chemerpils’ka areas by different geological organizations. Maximal platinum content (1 g/t) was explored in the Kapitans’kyi ultrabasic massif. However native platinum was detected just as inclusions in minerals-bearers. In 2009 native platinum was explored for the first time in individual grains in the Chemerpil’ska and Bakshyns’ka structures. Chemerpil’ska structure is an association of eight oval synclinal formations from 120 to 700 metres in length and with steep to subvertical limbs dip which consist of the Archean metabasites and siliceous-carbonate igneous-sedimentary rocks. Most of their cores have high content of magnetite, often of industrial contents. Native platinum is set in amphibolite which is pierced by thin (to 1 cm) veins of quartz and of the fissures with aggregates of sulfides and clay minerals on its side. Steel-grey platinum grains with metallic lustre have elongated lamellar shape. Their sizes are (mm): 0.3×0.1; 0.5×0.1; 0.5×0.4; 0.7×0.1; 0.75×0.2. Gold content in the samples with platinum is 0.32 g/t. Satellite elements are zinc, argentum, satellite minerals are arsenopyrite, molybdenite, pyrrhotine. Chemical composition of the native platinum is the next, %: Pt (97.185—99.693), Pd (0—0.019), Os (0,012—0,099), Rh (0,213— 0,309), Ni (0—0,009), Fe (0,009—0,023), Cu (0—0.008), Ag (0—0.007). Mineralogical researches point to the spatial connection between platinum and native gold. Materials for argumentation of genetic type of platinum mineralization of Chemerpil’ska structure are not sufficient to day. It is just possible to point out the connection of gold and platinum with deoxidated, scarning and greisening mafites. In the future it is necessary to continue geochemical and mineralogical researches of platinum mineralization of the Chemerpil’ska structure. It will promote a considerable growth of economic demand as the possible future deposit of noble metals.

Popovchenko S.E., Evtekhov V.D.Distribution of precious metals in the chromite-bearing weathering crusts Lipovenkovska group ultrabasites of Middle Pobuzhye// Journal of the Dnipropetrovsk University. Geology. Geography. - № 15. - 2014. - С. 42 – 48.

Studied geochemistry of gold, silver, platinum and palladium in the nontronitic weathering crusts by Middle Pobuzhye. The background concentrations and levels of geochemical anomalies, migration considerations for each of the metals in various zones of the weathering crust. The conclusion is drawn on their industrial prospects.Key words:geochemistry, nontronites, precious metal, weathering crust.

Yushin A.A. Prospect for platinoide-chromite mineralization in ultramafic complexes (Kapitanivske deposit, Middle Pobuzhye, taken as an example) // Geological and Mineralogical Journal of the KryvyiRih Technical University.KryvyiRih. - № 1. - 2003. -P. 34 – 38.

Chromite mineralization of Kapitanivske deposit is accompanied by gold and platinum mineralization. It is necessary to research in detail kapitanivsky type ores of Ukrainian shield for their complex utilization.

Syomka V.O., Bondarenko S.M., Pavlyuk V.M., Kornienko P.K., Bondarenko I.M. KapitankaOreField (Dniester-Bug Region of the Ukrainian Shield) // Mineralogical Journal. – 28, №2 (148). – 2006. – P. 94-107.

On the basis of geological-petrographic and ore-geochemical researches it is distinguished four types of rocks: 1 - intrusive (gabbro, gabbro-norites, norites), 2 - sedimentary (manganous dolomite), 3 - metasomatic (magnesian skarns), 4 - ultrametamorphic (plagiomigmatites, micaites, quartz veins, postgabbroic crystalloschists, pegmatitic granites). It is established gold-arsenic-sulfide (high-temperature) and gold-silver-sulfide (low-temperature) types of the mineralization, located in magnesian skarns.

Kulish E.O., Kalinin V.I. Ferrous metals. Chromium. Kapitanskoye deposit // Metallic minerals. Т 1. - Kiev-Lviv: Center of Europe. - 2005. -P. 152-154.

Bobrov A.B., Gurskiy D.S., Hoshovskyi et.al. Metallic rhenium in natural geological systems: the first world experience of description by the example of ultrabasic massifs of the Middle Pobuzhye (Ukrainian Shield) // Scientific proceedings of UkrSGRI. – № 2. – 2007. – P. 60-82.

Geological and structural position ofkapitanivsko-derenyukhynskiyultrabasitecomplexis given in the article. Features of Earth Crust deep framework of Golovanivska suture zone are considered. Geology of Pobuzka group serpentinitemassifs is described. Ore and petrological characteristic of Kapitanivskiy ultrabasic massif (Middle Pobuzhzhya) is represented. Description of new potential minable types of ore deposits were specified within the Kapitanivskiy massif for the first time. Native rhenium and platinum-group elements contained in sulphoarsenids such as osmium, iridium, ruthenium, rhodium and platinum were revealed as a result of mineragraphic, electron microscope and microprobe studies. At least two ore types of native rhenium and PGE within the Kapitanivskiy ore field are predicted by the preliminary data.